Abstract

This pilot study investigates the existence of seasonal movements of sheep – transhumance – in Iron Age Catalonia (North-Eastern Spain). The occurrence of seasonalmovement of livestock between the coast and the interior, perhaps in relation to the Mediterraneanmarket, was suggested for this area based on landscape and palynological studies. This hypothesis was tested on the basis of strontium, carbon and oxygen isotope analysis fromseven sheep lower third molars. The evidence obtained suggests that the animals did not move across geological areas during the time of enamelmineralization. In addition, the paper provides valuable isotopic evidence that can be used in further studies.